Soil texture
Soil texture refers to the proportion of different mineral particles, such as Sand, Silt, and Clay, in a given soil sample, which affects its physical and chemical properties. The texture of soil is determined by the size of the particles, with sand being the largest and clay being the smallest. This characteristic is crucial in Agricultural knowledge and Soil ecology, as it influences the soil's ability to retain water and nutrients, as well as its suitability for different types of plants. The Classification (statistics) of soil texture is often based on the percentage of sand, silt, and clay particles present. Understanding soil texture is essential for various applications, including Chemical analysis and Data mining in the field of Environmental science.